File:Chertified crinoid head in limestone (Fort Payne Formation, Lower Mississippian; Lake Cumberland, Kentucky, USA) (50669942703).jpg
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[edit]DescriptionChertified crinoid head in limestone (Fort Payne Formation, Lower Mississippian; Lake Cumberland, Kentucky, USA) (50669942703).jpg |
Fossiliferous limestone from the Mississippian of Kentucky, USA. The Fort Payne Formation of southern Kentucky is richly fossiliferous and is dominated by crinoids. Crinoids ("sea lilies") are sessile, benthic, filter-feeding, marine invertebrates that were abundant in Paleozoic oceans. The group nearly went extinct at the Permian-Triassic mass extinction 251 million years ago. Crinoids are not common in modern oceans - they are usually deep-water forms now, but some shallow-water forms also exist today. A crinoid is essentially a starfish on a stick. The stick, or stem, lifts the organism to a moderately high tier above the seafloor, which is conducive to non-competitive filter feeding. The flower-like "head" of the crinoid consists of numerous cemented calcite plates that surround the digestive system and other soft parts. The arms are feather-like and are the structures that engage in filter-feeding. In the fossil record, crinoid stems are common, whereas crinoid heads are uncommon to rare, because they disaggregate quickly after death. Individual pieces of a crinoid stem are called columnals - they are usually somewhat shaped like poker chips. Each columnal is composed of a single crystal of calcite (CaCO3 - calcium carbonate). The specimen seen here is a cross-section through a camerate crinoid head in limestone. The crinoid head itself has been replaced by cryptocrystalline quartz (SiO2) - this fossil preservation style is called "silicification", or in this case "chertification". A crinoid researcher has identified the crinoid head as Alloprosallocrinus conicus. Classification: Animalia, Echinodermata, Crinoidea, Camerata, Monobathrida, Composcrinina, Batocrinidae Stratigraphy: Fort Payne Formation, Osagean Stage/Series, upper Lower Mississippian Locality: lakeside exposure at the western-most tip of Cave Springs Ridge, southwestern-most end of Wolf Creek arm of central Lake Cumberland, southeastern Russell County, southern Kentucky, USA |
Date | |
Source | Chertified crinoid head in limestone (Fort Payne Formation, Lower Mississippian; Lake Cumberland, Kentucky, USA) |
Author | James St. John |
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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/50669942703. It was reviewed on 20 January 2022 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0. |
20 January 2022
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current | 00:13, 20 January 2022 | 2,142 × 1,526 (2.5 MB) | SeichanGant (talk | contribs) | Transferred from Flickr via #flickr2commons |
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Camera manufacturer | Canon |
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Camera model | Canon PowerShot D10 |
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F-number | f/11 |
ISO speed rating | 80 |
Date and time of data generation | 16:30, 27 November 2020 |
Lens focal length | 11.614 mm |
Width | 4,000 px |
Height | 3,000 px |
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Pixel composition | RGB |
Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 180 dpi |
Vertical resolution | 180 dpi |
Software used | Adobe Photoshop Elements 18.0 (Macintosh) |
File change date and time | 22:45, 1 December 2020 |
Y and C positioning | Co-sited |
Exif version | 2.21 |
Date and time of digitizing | 16:30, 27 November 2020 |
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Image compression mode | 3 |
APEX shutter speed | 5.90625 |
APEX aperture | 6.90625 |
APEX exposure bias | −0.66666666666667 |
Maximum land aperture | 4 APEX (f/4) |
Metering mode | Pattern |
Flash | Flash fired, compulsory flash firing, red-eye reduction mode |
Supported Flashpix version | 1 |
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Sensing method | One-chip color area sensor |
File source | Digital still camera |
Custom image processing | Normal process |
Exposure mode | Manual exposure |
White balance | Auto white balance |
Digital zoom ratio | 1 |
Scene capture type | Standard |
Lens used | 6.2-18.6 mm |
Date metadata was last modified | 17:45, 1 December 2020 |
Unique ID of original document | 63A1CB39CBE1E7A22B6D978C2FB12F74 |
IIM version | 53,248 |